
Kleiman Pump & Well Drilling Inc
Iron Mountain, MI49801-0704
Typical Niagara area geology: surficial sand/gravel overlying granite bedrock. Residential wells typically reach granite at 20–45 ft, with wells drilled 100–225+ ft for consistent supply.
Showing contractors within 60 miles of Niagara. 10 results found.
A geological estimate for the Niagara area.
Typical Well Depth
Static Water Level
Recommended Method
In the Niagara, WI region, well logs consistently show an upper sequence of unconsolidated sand and gravel ranging from about 8 to 72 feet, commonly 20–45 feet thick. This is typically underlain by granite or hard rock, which forms the primary aquifer below these unconsolidated deposits. Wells for residential use (5–15+ GPM) are generally cased through the sand/gravel into or just past the granite, seldom exceeding 150–225 feet total depth. High-capacity or low-yield sites may go deeper into the granite. Casing is usually set at the base of the unconsolidated material (35–45 ft). Static water levels are generally 18–25 ft below ground surface, and rotary mud circulation is the dominant drilling method. Grout is primarily cement, sealing surface to casing depth.
Depth (Feet) | Formation Type | Description | Characteristics |
---|---|---|---|
0 – 35 ft | Sand and Gravel | Unconsolidated sand (often with gravel/cobble, sometimes clay or silt interbeds); typically yellow/dirty to clean, soft-caving. | Color: Yellow, grey, or dirty Hardness: Soft |
35 – 145 ft | Granite/Hard Rock | Crystalline granite or very hard bedrock; major aquifer zone for most wells. | Color: Grey or black Hardness: Hard |